Australasian Fossils: A Students' Manual of PalaeontologyChapman, Frederick
Science
Australasian Fossils: A Students' Manual of Palaeontology
Chapman, Frederick
Paleontology -- Australia
A species of the Astraeidae (Star-corals) of the reef-forming section,
_Plesiastraea st.vincenti_, is found in the Kalimnan of Hallett's Cove,
South Australia.
_HYDROZOA._
The few animals of this group met with in fossil faunas are represented by
the living _Millepora_ (abundant as a coral reef organism), _Hydractinia_
(parasitic on shells, etc.), and _Sertularia_ (Sea-firs).
=Milleporids and Stylasterids.--=
Although so abundant at the present time, the genus _Millepora_ does
not date back beyond the Pleistocene. The Eocene genus _Axopora_ is
supposed to belong here, but is not Australian. Of the Stylasterids one
example is seen in _Deontopora_, represented by the branchlets of _D.
mooraboolensis_, from the Janjukian limestone of the Moorabool Valley,
near Geelong.
=Hydractinia.--=
_Hydractinia_ dates from the Upper Cretaceous rocks in England, and in
Australia its encrusting polypidom is found attached to shells in the
polyzoal limestone of Mount Gambier (Miocene).
Stromatoporoids.
An important group of reef-builders in Palaeozoic times was the organism
known as _Stromatopora_, and its allies. The structures of these hydroid
polyps resemble successional and repetitional stages of a form like
_Hydractinia_. As in that genus it always commenced to grow upon a base
of attachment such as a shell, increasing by successive layers, until the
organic colony often reached an enormous size, and formed great mounds
and reefs (see _antea_, Fig. 32). The stromatoporoid structure was formed
by a layer of polyp cells separated by vertical partitions, upon which
layer after layer was added until a great vertical thickness was attained.
This limestone-making group first appeared in the Silurian, and probably
reached its maximum development in Middle Devonian times, when it almost
disappeared, except to be represented in Carbopermian strata by a few
diminutive forms.
[Illustration: =Fig. 72.--STROMATOPOROIDEA and CLADOPHORA.=
A--Actinostroma clathratum, Nich. Devonian. Rough Range, W.A.
B--Actinostroma clathratum, Nich. Devonian. Rough Range, W.A. Vertical
section.
(_After G. J. Hinde_).
C--Callograptus sp. Up. Ordovician. San Remo, Vict.
(_After T. S. Hall_).
D--Ptilograptus sp. Up. Ordovician. San Remo, Vict.
(_After T. S. Hall_).
E--Dictyonema pulchellum, T. S. Hall. L. Ordov. Lancefield, Vict.
F--Dictyonema macgillivrayi, T. S. Hall. L. Ordov. Lancefield, Vict.
]
=Silurian Stromatoporoids.--=
In the Silurian limestones of Victoria (Lilydale, Waratah Bay, Walhalla
and Loyola), and New South Wales (near Yass), Stromatoporoids belonging to
the genera _Clathrodictyon_ (probably _C. regulare_), _Stromatopora_ and
_Idiostroma_ occur. _Stromatoporella_ has been recorded from the Silurian
rocks of the Jenolan Caves, New South Wales.
=Devonian Stromatoporids.--=
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